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Hurricane Cindy impacted the Carolinas, the Mid-Atlantic states, New England, and the Canadian Maritime Provinces during the 1959 Atlantic hurricane season. The third storm of the season, Cindy originated from a low-pressure area associated with a cold front located east of northern Florida. The low developed into a tropical depression on July 5 while tracking north-northeastward, and became Tropical Storm Cindy by the next day. Cindy turned westward because of a high-pressure area positioned to its north, and further intensified into a weak hurricane off the coast of the Carolinas on July 8. Early on July 9, Cindy made landfall near McClellanville, South Carolina, and re-curved to the northeast along the Fall Line as a tropical depression. It re-entered the Atlantic on July 10, quickly re

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  • Hurricane Cindy impacted the Carolinas, the Mid-Atlantic states, New England, and the Canadian Maritime Provinces during the 1959 Atlantic hurricane season. The third storm of the season, Cindy originated from a low-pressure area associated with a cold front located east of northern Florida. The low developed into a tropical depression on July 5 while tracking north-northeastward, and became Tropical Storm Cindy by the next day. Cindy turned westward because of a high-pressure area positioned to its north, and further intensified into a weak hurricane off the coast of the Carolinas on July 8. Early on July 9, Cindy made landfall near McClellanville, South Carolina, and re-curved to the northeast along the Fall Line as a tropical depression. It re-entered the Atlantic on July 10, quickly restrengthening into a tropical storm while it began to move faster. On July 11, Cindy passed over Cape Cod, while several other weather systems helped the storm maintain its intensity. Cindy transitioned into an extratropical cyclone on July 12 as it neared the Canadian Maritime Provinces. Overall the structural damage from Cindy was minimal. One driver was killed in Georgetown, South Carolina after colliding with a fallen tree, and five indirect deaths were caused by poor road conditions wrought by the storm in New England. Many areas experienced heavy rains, and several thousand people evacuated. Other than broken tree limbs, shattered windows and power outages, little damage occurred. Cindy brought a total of eleven tornadoes with it, of which two caused minor damage in North Carolina. The heaviest rainfall occurred in north central South Carolina, where rainfall amounted to 9.79 inches (249 mm). Tides ranged from 1 to 4 feet (0.30 to 1.22 m) above normal along the coast. As drought-like conditions were present in the Carolinas at the time, the rainfall produced by Hurricane Cindy in the area was beneficial. After becoming extratropical over the Canadian Maritimes, the cyclone produced heavy rains and strong winds that sunk one ship. Damage caused by Cindy was estimated at $75,000 (1959 USD). (en)
  • O furacão Cindy afetou as Carolinas, os estados do Médio Atlântico, a Nova Inglaterra e as Províncias Marítimas do Canadá durante a temporada de furacões no Atlântico de 1959 . A terceira tempestade da temporada, Cindy, originou-se de uma área de baixa pressão associada a uma frente fria localizada a leste do norte da Flórida. A baixa evoluiu para uma depressão tropical em 5 de julho, enquanto seguia para o norte-nordeste, e se tornou a tempestade tropical Cindy no dia seguinte. Cindy virou para o oeste por causa de uma área de alta pressão posicionada ao norte, e se intensificou ainda mais em um furacão fraco na costa das Carolinas em 8 de julho. No início de 9 de julho, Cindy atingiu a costa perto de McClellanville, Carolina do Sul, e fez uma nova curva para o nordeste ao longo da Fall Line como uma depressão tropical. Ele reentrou no Atlântico em 10 de julho, rapidamente se fortalecendo em uma tempestade tropical enquanto começava a se mover mais rápido. Em 11 de julho, Cindy passou por Cape Cod, enquanto vários outros sistemas climáticos ajudaram a tempestade a manter a sua intensidade . Cindy fez a transição para um ciclone extratropical em 12 de julho, quando se aproximou das províncias marítimas canadenses . O dano estrutural geral de Cindy foi mínimo. Um motorista morreu em Georgetown, Carolina do Sul, após colidir com uma árvore caída, e cinco mortes indiretas foram causadas por más condições das estradas causadas pela tempestade na Nova Inglaterra. Muitas áreas sofreram fortes chuvas e vários milhares de pessoas foram evacuadas. Além de ramos de árvores quebrados, janelas quebradas e apagões, poucos danos ocorreram. Cindy trouxe um total de onze tornados com ele, dos quais dois causaram danos menores na Carolina do Norte. As chuvas mais fortes ocorreram no centro-norte da Carolina do Sul, onde as chuvas somaram 9,79 polegadas (249 mm). As marés variaram de 1 a 4 pés (0,30 a 1,2 m) acima do normal ao longo da costa. Como as condições semelhantes às da seca estavam presentes nas Carolinas na época, as chuvas produzidas pelo furacão Cindy na área foram benéficas. Depois de se tornar extratropical nas Marítimas canadenses, o ciclone produziu fortes chuvas e ventos fortes que afundaram um navio. Os danos causados por Cindy foram estimados em $ 75.000 (1959 USD). (pt)
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  • Hurricane Cindy impacted the Carolinas, the Mid-Atlantic states, New England, and the Canadian Maritime Provinces during the 1959 Atlantic hurricane season. The third storm of the season, Cindy originated from a low-pressure area associated with a cold front located east of northern Florida. The low developed into a tropical depression on July 5 while tracking north-northeastward, and became Tropical Storm Cindy by the next day. Cindy turned westward because of a high-pressure area positioned to its north, and further intensified into a weak hurricane off the coast of the Carolinas on July 8. Early on July 9, Cindy made landfall near McClellanville, South Carolina, and re-curved to the northeast along the Fall Line as a tropical depression. It re-entered the Atlantic on July 10, quickly re (en)
  • O furacão Cindy afetou as Carolinas, os estados do Médio Atlântico, a Nova Inglaterra e as Províncias Marítimas do Canadá durante a temporada de furacões no Atlântico de 1959 . A terceira tempestade da temporada, Cindy, originou-se de uma área de baixa pressão associada a uma frente fria localizada a leste do norte da Flórida. A baixa evoluiu para uma depressão tropical em 5 de julho, enquanto seguia para o norte-nordeste, e se tornou a tempestade tropical Cindy no dia seguinte. Cindy virou para o oeste por causa de uma área de alta pressão posicionada ao norte, e se intensificou ainda mais em um furacão fraco na costa das Carolinas em 8 de julho. No início de 9 de julho, Cindy atingiu a costa perto de McClellanville, Carolina do Sul, e fez uma nova curva para o nordeste ao longo da Fall L (pt)
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  • Hurricane Cindy (1959) (en)
  • Furacão Cindy (1959) (pt)
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